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Published in 2020 at "Tectonophysics"
DOI: 10.1016/j.tecto.2020.228502
Abstract: Abstract Characterizing the inelastic strain field around co-seismic faults is a key to understanding earthquake rupture processes. We aim to detect zones of inelastic deformation around surface ruptures, using Anisotropy of Magnetic Susceptibility (AMS) analyses.…
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Keywords:
zones inelastic;
deformation around;
inelastic deformation;
surface ruptures ... See more keywords